2. UNIT SIX: Earth’s Structure  Chapter 18 Earth’s History and Rocks  Chapter 19 Changing Earth  Chapter 20 Earthquakes and Volcanoes

4. Chapter Nineteen: Changing Earth  19.1 Inside Earth  19.2 Plate Tectonics  19.3 Plate Boundaries  19.4 Metamorphic Rocks

5. 19.4 Learning Goals  Define metamorphism.  Identify characteristics of metamorphic rocks.  Differentiate between regional and contact metamorphism.

6. 19.4 Metamorphic Rocks  The word metamorphic means “changed form.”  A metamorphic rock is a rock formed from another kind of rock due to heat and pressure.

7. 19.4 Metamorphic rock  Large-scale metamorphic events, called regional metamorphism, occur when lithospheric plates subduct or collide.

8. 19.4 Metamorphic rocks  When magma comes in contact with another type of rock, the high heat may form metamorphic rock near the point of contact.  This is called contact metamorphism.

9. 19.4 Metamorphic rocks  Limestone is a rock made of shells.  During contact metamorphism limestone becomes marble under heat and pressure.

10. 19.4 Metamorphic rocks  High-grade metamorphism involves high pressure and either low or high temperatures.  In this process, the minerals in a rock change to form new minerals.

12. 19.4 Changing rocks

13. 19.4 Metamorphic rocks  Heat and pressure result when colliding continents form mountains at a convergent boundary.  Mountains are where we find metamorphic rocks.

14. 19.4 Metamorphic rocks tell great stories  Geologists use rocks as clues to understand the history of Earth.

15. Mass Extinction:  At the end of the Cretaceous Period, almost all of Earth’s large vertebrates (including the dinosaurs), and most of the oceans’ plankton became extinct. Research is currently underway to find out what caused this mass extinction. Devastation and Opportunity